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pmip3:wg:degla:bc:core [2015/02/18 12:45]
ruza [Proposal]
pmip3:wg:degla:bc:core [2015/02/18 14:01]
ruza
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       * **CH<​sub>​4</​sub>​** from [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06950.html | Loulergue et al. (2008)]]<​sup>​[5]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.       * **CH<​sub>​4</​sub>​** from [[http://​www.nature.com/​nature/​journal/​v453/​n7193/​full/​nature06950.html | Loulergue et al. (2008)]]<​sup>​[5]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.
       * **N<​sub>​2</​sub>​O** from [[http://​www.sciencedirect.com/​science/​article/​pii/​S0012821X10006023 | Schilt et al. (2010)]]<​sup>​[6]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.       * **N<​sub>​2</​sub>​O** from [[http://​www.sciencedirect.com/​science/​article/​pii/​S0012821X10006023 | Schilt et al. (2010)]]<​sup>​[6]</​sup>​ on the AICC2012 timescale of [[http://​www.clim-past.net/​9/​1733/​2013/​cp-9-1733-2013.html | Veres et al. (2013)]]<​sup>​[3]</​sup>​.
-  * **Ice sheets**: Choice of either ICE6G_C<​sup>​[7-8]</​sup>​ or Lev Tarasov'​s global reconstruction of ice sheet evolution. \\ Whichever is chosen for the LGM should be kept for the whole simulation. \\ [See the [[pmip3:​wg:​degla:​bc:​ice | last deglaciation ice sheets]] page for more information on the ice sheets.]+  * **Ice sheets**: Choice of either ​the [[pmip3:​wg:​degla:​bc:​ice#​ice6g_c_reconstruction | ICE6G_C]]<​sup>​[7-8]</​sup>​ or [[pmip3:​wg:​degla:​bc:​ice#​lev_tarasov_s_reconstruction | Lev Tarasov'​s]]<​sup>​[9-12]</​sup> ​global reconstruction of ice sheet evolution. \\ Whichever is chosen for the LGM should be kept for the whole simulation. \\ [See the [[pmip3:​wg:​degla:​bc:​ice | last deglaciation ice sheets]] page for more information on the ice sheets.]
   * **Meltwater**:​ __no meltwater__ in the core. ((Global meltwater fluxes that are consistent with the ice sheet reconstructions will be provided for alternative simulations to the core, but must not be used for the core.)) ​   * **Meltwater**:​ __no meltwater__ in the core. ((Global meltwater fluxes that are consistent with the ice sheet reconstructions will be provided for alternative simulations to the core, but must not be used for the core.)) ​
   * Other boundary conditions: keep as per the LGM. \\ \\   * Other boundary conditions: keep as per the LGM. \\ \\
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   - Schilt, A. et al. Atmospheric nitrous oxide during the last 140,000 years. Earth Planet. Sci. Lett. 300, 33–43 (2010).   - Schilt, A. et al. Atmospheric nitrous oxide during the last 140,000 years. Earth Planet. Sci. Lett. 300, 33–43 (2010).
   - Argus, D. F., Peltier, W. R., Drummond, R. & Moore, A. W. The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning,​ exposure age dating of ice thicknesses,​ and relative sea level histories. Geophys. J. Int. ggu140 (2014).   - Argus, D. F., Peltier, W. R., Drummond, R. & Moore, A. W. The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning,​ exposure age dating of ice thicknesses,​ and relative sea level histories. Geophys. J. Int. ggu140 (2014).
-  - Peltier, W. R., Argus, D. F. & Drummond, R. Space geodesy constrains ice age terminal deglaciation:​ The global ICE-6G_C (VM5a) model. J. Geophys. Res. Solid Earth 2014JB011176 (2015). \\ \\+  - Peltier, W. R., Argus, D. F. & Drummond, R. Space geodesy constrains ice age terminal deglaciation:​ The global ICE-6G_C (VM5a) model. J. Geophys. Res. Solid Earth 2014JB011176 (2015). 
 +  -  Tarasov, L. & Peltier, W. R. Greenland glacial history and local geodynamic consequences. Geophys. J. Int. 150, 198–229 (2002). 
 +  - Tarasov, L., Dyke, A. S., Neal, R. M. & Peltier, W. R. A data-calibrated distribution of deglacial chronologies for the North American ice complex from glaciological modeling. Earth Planet. Sci. Lett. 315–316, 30–40 (2012) 
 +  - Briggs, R. D., Pollard, D. & Tarasov, L. A data-constrained large ensemble analysis of Antarctic evolution since the Eemian. Quat. Sci. Rev. 103, 91–115 (2014). 
 +  - Tarasov et al. Eurasian ice sheet evolution (in prep.).\\ \\
  
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pmip3/wg/degla/bc/core.txt · Last modified: 2015/10/21 13:26 by ruza